JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT

The intimate stratigraphical association between Lower Toarcian manganese carbonates and carbon-rich shales in Austria, Czechoslovakia, Germany, Hungary, Italy, and Switzerland is suggestive of a genetic connection between the two, given the similar anoxic to euxinic depositional environments in whi...

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Main Authors: Jenkyns, H, Geczy, B, Marshall, J
Format: Journal article
Language:English
Published: 1991
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author Jenkyns, H
Geczy, B
Marshall, J
author_facet Jenkyns, H
Geczy, B
Marshall, J
author_sort Jenkyns, H
collection OXFORD
description The intimate stratigraphical association between Lower Toarcian manganese carbonates and carbon-rich shales in Austria, Czechoslovakia, Germany, Hungary, Italy, and Switzerland is suggestive of a genetic connection between the two, given the similar anoxic to euxinic depositional environments in which both these distinctive sediments form today. Ammonite biostratigraphy and carbon-isotope stratigraphy suggest that these metalliferous deposits are everywhere of identical age, namely tenuicostatum to early falciferum Zones. Recognition of an early Toarcian anoxic event in the Alpine-Mediterranean domain, characterized by the development of a well-developed oxygen-minimum zone across the rifted proto-continental margins of the Tethys, indicates that these metalliferous deposits can be related to mid-water transport of manganese, possibly of continental derivation. -from Authors
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spelling oxford-uuid:da6b2c7a-1ff5-4e88-ab05-8af625b154572022-03-27T09:03:10ZJURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENTJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:da6b2c7a-1ff5-4e88-ab05-8af625b15457EnglishSymplectic Elements at Oxford1991Jenkyns, HGeczy, BMarshall, JThe intimate stratigraphical association between Lower Toarcian manganese carbonates and carbon-rich shales in Austria, Czechoslovakia, Germany, Hungary, Italy, and Switzerland is suggestive of a genetic connection between the two, given the similar anoxic to euxinic depositional environments in which both these distinctive sediments form today. Ammonite biostratigraphy and carbon-isotope stratigraphy suggest that these metalliferous deposits are everywhere of identical age, namely tenuicostatum to early falciferum Zones. Recognition of an early Toarcian anoxic event in the Alpine-Mediterranean domain, characterized by the development of a well-developed oxygen-minimum zone across the rifted proto-continental margins of the Tethys, indicates that these metalliferous deposits can be related to mid-water transport of manganese, possibly of continental derivation. -from Authors
spellingShingle Jenkyns, H
Geczy, B
Marshall, J
JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT
title JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT
title_full JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT
title_fullStr JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT
title_full_unstemmed JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT
title_short JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT
title_sort jurassic manganese carbonates of central europe and the early toarcian anoxic event
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